← NS-DCRP / DCRP-35 · DSS Enstrophy Replenishment and Outer Affine-Jet Reduction
Replaces DCRP-34's heuristic language with exact vorticity/enstrophy dynamical bookkeeping, proves that a nonzero strictly-DSS core must be sustained by positive vortex stretching or inward enstrophy transport, localizes the unavoidable stretching source to a finite intermediate annular region, and reduces it to a finite-dimensional symmetric trace-free affine strain jet.
Relationship to the rest of the series, stated as closely as possible in the document's own words, not my interpretation.
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